Cheshire Basin

E105018

The Cheshire Basin is a large geological sedimentary basin in northwest England known for its thick Triassic rock sequences and associated salt deposits.

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All labels observed (2)

Label Occurrences
Cheshire Basin canonical 1
Mersey Basin 1

Statements (49)

Predicate Object
instanceOf geological basin
sedimentary basin
age Mesozoic
boundedBy Midland Platform
Pennines
Welsh Massif
contains Mercia Mudstone Group
Northwich salt field
surface form: Middlewich salt field

Nantwich salt field
Northwich salt field
Sherwood Sandstone Group
Triassic evaporites
Triassic mudstones
Triassic sandstones
Northwich salt field
surface form: Winsford salt field

salt-related subsidence features
subsidence hollows
country United Kingdom
depositionalEnvironment continental fluvial
playa lake
sabkha evaporitic
drainage River Dee
River Mersey
River Weaver
economicActivity brine extraction
salt mining
extendsInto Greater Manchester
Merseyside
Shropshire
Staffordshire
formedBy Mesozoic crustal extension
geologicalPeriod Triassic
hasMaximumThickness over 2 kilometres of Triassic strata
knownFor evaporite deposits
halite beds
salt deposits
thick Triassic rock sequences
locatedIn Cheshire
North West England
surface form: northwest England
majorResource brine
rock salt
notableTownWithin Middlewich
Nantwich
Northwich
Winsford
overlies Carboniferous rocks
partOf East Irish Sea Basin system
tectonicSetting extensional basin
underlainBy Permian rocks

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Cheshire Plain partOf Cheshire Basin
St Helens locatedOn Cheshire Basin
this entity surface form: Mersey Basin